On the eastern periphery, in summer, the West Greenland Current transports water from the Atlantic Ocean to the North.
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It is initiated by the East Greenland Current and continued by the West Greenland Current, which brings warmer, more saline waters northwards, along the Greenland coasts up to the Baffin Bay.
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The sea is rich in fish and invertebrates, especially in the milder West Greenland Current, and a large part of the Greenland fauna associated with marine production, including large colonies of seabirds.
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In January 2010, the Gulf Stream briefly connected with the West Greenland Current after fluctuating for a few weeks due to an extreme negative phase of the Arctic oscillation, temporarily diverting it west of Greenland.
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For an extended time, nonetheless, the relatively warm West Greenland current flowing northwards along the southwestern coast of Greenland made it feasible for the Norse to farm much as their relatives did in Iceland or northern Norway.
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